| Article ID | Journal | Published Year | Pages | File Type | 
|---|---|---|---|---|
| 6443585 | Gondwana Research | 2012 | 18 Pages | 
Abstract
												⺠The Bitlis Massif in SE Turkey is intruded by leucocratic magmas represented by the DoÄruyol metagranite at ~ 572 Ma. ⺠The meta-granite crystallised from calc-alkaline, I-type, peraluminous arc-type melts. ⺠Zircon age data show maximum depositional age of ~ 627 Ma (paragneiss) and ~ 520 Ma (metagranite) for regional Pan-African metamorphism.
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											Authors
												P. Ayda Ustaömer, Timur Ustaömer, Axel Gerdes, Alastair H.F. Robertson, Alan S. Collins, 
											